Chemical characteristics of haze particles in Xi'an during Chinese Spring Festival: Impact of fireworks burning

被引:8
|
作者
Can Wu [1 ,2 ]
Gehui Wang [1 ,3 ,4 ,2 ]
Jiayuan Wang [1 ]
Jianjun Li [1 ]
Yanqin Ren [1 ,5 ]
Lu Zhang [1 ]
Cong Cao [1 ,2 ]
Jin Li [1 ,2 ]
Shuagshuang Ge [3 ]
Yuning Xie [3 ]
Xinpei Wang [3 ]
Guoyan Xue [3 ]
机构
[1] State Key Laboratory of Loess and Quaternary Geology, Key Lab of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Academy of Sciences
[2] University of Chinese Academy of Sciences
[3] Key Laboratory of Geographic Information Science of the Ministry of Education, School of Geographic Sciences, East China Normal University
[4] Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences
[5] State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences
基金
国家重点研发计划;
关键词
Inorganic ions; Aerosol acidity; Liquid water content; Composition and source; Nitrate formation;
D O I
暂无
中图分类号
X513 [粒状污染物];
学科分类号
0706 ; 070602 ;
摘要
Fireworks burning releases massive fine particles and gaseous pollutants, significantly deteriorating air quality during Chinese Lunar New Year(LNY) period. To investigate the impact of the fireworks burning on the atmospheric aerosol chemistry, 1-hr time resolution of PM2.5samples in Xi’an during the winter of 2016 including the LNY were collected and detected for inorganic ions, acidity and liquid water content(LWC) of the fine aerosols. PM2.5during the LNY was 167 ± 87 μg/m~3, two times higher than the China National Ambient Air Quality Standard(75 μg/m~3). K~+(28 wt.% of the total ion mass) was the most abundant ion in the LNY period, followed by SO42-(25 wt.%) and Cl-(18 wt.%). In contrast, NO3~-(34 wt.%) was the most abundant species in the haze periods(hourly PM32-2.5> 75 μg/m), followed by SO4(29.2 wt.%) and NH4~+(16.3 wt.%), while SO42-(35 wt.%) was the most abundant species in the clean periods(hourly PM2.5< 75 μg/m~3), followed by NO3~-(23.1 wt.%) and NH4~+(11 wt.%). Being different from the acidic nature in the non-LNY periods, aerosol in the LNY period presented an alkaline nature with a pH value of 7.8 ± 1.3. LWC during the LNY period showed a robust linear correlation with K2SO4and KCl, suggesting that aerosol hygroscopicity was dominated by inorganic salts derived from fireworks burning. Analysis of correlations between the ratios of NO--3/SO42-and NH4~+/SO42-indicated that heterogeneous reaction of HNO3with NH3was an important formation pathway of particulate nitrate and ammonium during the LNY period.
引用
收藏
页码:179 / 187
页数:9
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